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� ; <br /> August 25,2006 <br /> Nir. Scott Anderson <br /> I,&A Job No. 6A 126 <br /> Page 3 <br /> medium-dense state, and is moderatcly permeable and compressible. The underlying fresh till is <br /> very dense and is practically impervious to stormwater infiltration. The fresh till has the strength <br /> of low-grade concrete and can stand in a steep natuial or cut slope for a long period. If remains <br /> undisturbed nnd well-drained, the fresh till can provide ezcellent foundation support with little <br /> setticment expected. <br /> The advance outwnsh soil unit underlying the Vashon tilf is composed of stratified sand and <br /> gmvel with minor�unounts of silt und clay, deposited by the meltwater of advancing glacial ice. <br /> Due to their generally granulaz composition, the advance outwash deposits are of modecately <br /> high pertneabiliry and generally drains fairly well. The advance outwash deposits are glacially <br /> overcidden and aze generally dense to very densc in its natw�il, undisturbed state, except the top 2 <br /> to 4 feet where exposcd on slopes which ma� be weathered to a loose to medium-dense state. <br /> The adva��ce outwash deFwsits can stand in stcep cuts or natural slopes for extended period when <br /> undisturbed. Where exposed on slopes with poor vegetation cover and subject to storm runoff or <br /> groundwater seepage, the advance outwash deposits can be gradually eroded and may slough and <br /> redeposit to a flatter inclination. The undedying fresh advance outwash deposits in iheir native, <br /> undisturbed state can rrovidc good foundation support with litile settlement expected for light to <br /> moderate residential structures. <br /> A steel T-bar was manually pushed into the surficial soils from the east boundary of the site to <br /> the crest of the steep slo� in the westem portion of the site to get an indication of the density or <br /> consistency of the soils. The probe could penetrate to about 6 to 10 ii..hes in the front yard and <br /> to nbout two fcet in the backyard. 11�e g�ound probing results indicate that the site is most likcly <br /> underlain by very-dense, Cresh till soils at very shallow depQ�. <br /> LIU & ASSOCIATES, INC. <br />